Comment on C. Covey: Atmospheric and oceanic heat transport simulations versus observations

1989 ◽  
Vol 15 (3) ◽  
Author(s):  
Claes Rooth
Keyword(s):  
Heat Transport ◽  
Oceanic Heat Transport

scholarly journals An oceanic heat transport pathway to the Amundsen Sea Embayment

2016 ◽  
Vol 121 (5) ◽  
pp. 3337-3349 ◽  
Author(s):  
Angelica R. Rodriguez ◽  
Matthew R. Mazloff ◽  
Sarah T. Gille
Keyword(s):  
Heat Transport ◽  
Transport Pathway ◽  
Amundsen Sea ◽  
Oceanic Heat Transport

Circulation and Modification of Warm Deep Water on the Central Amundsen Shelf

2014 ◽  
Vol 44 (5) ◽  
pp. 1493-1501 ◽  
Author(s):  
H. K. Ha ◽  
A. K. Wåhlin ◽  
T. W. Kim ◽  
S. H. Lee ◽  
J. H. Lee ◽  
...  
Keyword(s):  
Heat Transport ◽  
Deep Water ◽  
Shelf Area ◽  
Amundsen Sea ◽  
Glacial Ice ◽  
Ice Shelves ◽  
Oceanic Heat Transport ◽  
Eastern Side ◽  
Warm Deep Water ◽  
Western Side

Abstract The circulation pathways and subsurface cooling and freshening of warm deep water on the central Amundsen Sea shelf are deduced from hydrographic transects and four subsurface moorings. The Amundsen Sea continental shelf is intersected by the Dotson trough (DT), leading from the outer shelf to the deep basins on the inner shelf. During the measurement period, warm deep water was observed to flow southward on the eastern side of DT in approximate geostrophic balance. A northward outflow from the shelf was also observed along the bottom in the western side of DT. Estimates of the flow rate suggest that up to one-third of the inflowing warm deep water leaves the shelf area below the thermocline in this deep outflow. The deep current was 1.2°C colder and 0.3 psu fresher than the inflow, but still warm, salty, and dense compared to the overlying water mass. The temperature and salinity properties suggest that the cooling and freshening process is induced by subsurface melting of glacial ice, possibly from basal melting of Dotson and Getz ice shelves. New heat budgets are presented, with a southward oceanic heat transport of 3.3 TW on the eastern side of the DT, a northward oceanic heat transport of 0.5–1.6 TW on the western side, and an ocean-to-glacier heat flux of 0.9–2.53 TW, equivalent to melting glacial ice at the rate of 83–237 km3 yr−1. Recent satellite-based estimates of basal melt rates for the glaciers suggest comparable values for the Getz and Dotson ice shelves.

scholarly journals The impact of oceanic heat transport on the atmospheric circulation

2015 ◽  
Vol 6 (2) ◽  
pp. 591-615 ◽  
Author(s):  
M.-A. Knietzsch ◽  
A. Schröder ◽  
V. Lucarini ◽  
F. Lunkeit
Keyword(s):  
Entropy Production ◽  
Heat Transport ◽  
Atmospheric Circulation ◽  
General Circulation ◽  
Climate System ◽  
Hadley Cell ◽  
Near Surface ◽  
Oceanic Heat Transport ◽  
The Impact ◽  
Global Mean

Abstract. A general circulation model of intermediate complexity with an idealized Earth-like aquaplanet setup is used to study the impact of changes in the oceanic heat transport on the global atmospheric circulation. Focus is on the atmospheric mean meridional circulation and global thermodynamic properties. The atmosphere counterbalances to a large extent the imposed changes in the oceanic heat transport, but, nonetheless, significant modifications to the atmospheric general circulation are found. Increasing the strength of the oceanic heat transport up to 2.5 PW leads to an increase in the global mean near-surface temperature and to a decrease in its equator-to-pole gradient. For stronger transports, the gradient is reduced further, but the global mean remains approximately constant. This is linked to a cooling and a reversal of the temperature gradient in the tropics. Additionally, a stronger oceanic heat transport leads to a decline in the intensity and a poleward shift of the maxima of both the Hadley and Ferrel cells. Changes in zonal mean diabatic heating and friction impact the properties of the Hadley cell, while the behavior of the Ferrel cell is mostly controlled by friction. The efficiency of the climate machine, the intensity of the Lorenz energy cycle and the material entropy production of the system decline with increased oceanic heat transport. This suggests that the climate system becomes less efficient and turns into a state of reduced entropy production as the enhanced oceanic transport performs a stronger large-scale mixing between geophysical fluids with different temperatures, thus reducing the available energy in the climate system and bringing it closer to a state of thermal equilibrium.

Possible role of oceanic heat transport in Early Eocene climate

1995 ◽  
Vol 10 (2) ◽  
pp. 347-356 ◽  
Author(s):  
L. Cirbus Sloan ◽  
James C. G. Walker ◽  
T. C. Moore
Keyword(s):  
Heat Transport ◽  
Early Eocene ◽  
Oceanic Heat Transport

Northward oceanic heat transport in the main branch of the Norwegian Atlantic Current over the late Holocene

The Holocene ◽  
2017 ◽  
Vol 27 (7) ◽  
pp. 1034-1044 ◽  
Author(s):  
Andrea D Tegzes ◽  
Eystein Jansen ◽  
Torbjørn Lorentzen ◽  
Richard J Telford
Keyword(s):  
Heat Transport ◽  
Time Scales ◽  
Late Holocene ◽  
Meridional Overturning Circulation ◽  
The Arctic ◽  
Upper Ocean ◽  
Oceanic Heat Transport ◽  
The Past ◽  
Norwegian Margin ◽  
Atlantic Current

The Norwegian Atlantic Current represents the northernmost reaches of the (sub)surface limb of the Atlantic Meridional Overturning Circulation. Its shelf-edge branch, the Norwegian Atlantic Slope Current (NwASC), is of particular interest as it seems to be the main conduit for advected heat towards the Arctic. The objective of this study was to investigate northward oceanic heat transport in the NwASC on longer, geologically meaningful time scales. To this end, we reconstructed variations in the strength of the NwASC over the late Holocene using the sortable-silt method. We then analysed the statistical relationship between our palaeo-flow reconstructions and published upper-ocean hydrography proxy records from the same location on the mid-Norwegian Margin. Our sortable-silt time series show prominent multi-decadal to multi-centennial variability, but no clear long-term trend over the past 4200 years. These records we thus interpret to represent perturbations in a relatively stable late-Holocene mean flow. Our in-depth statistical analysis indicates that upper-ocean temperatures at the mid-Norwegian Margin may have varied independently from the strength of the NwASC on multi-decadal to multi-centennial time scales over the past few millennia.

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